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From May 4–6, 2007, a major and damaging tornado outbreak significantly affected portions of the Central United States.The most destructive tornado in the outbreak occurred on the evening of May 4 in western Kansas, where about 95% of the city of Greensburg in Kiowa County was destroyed by an EF5 tornado, the first of the new Enhanced Fujita Scale and such intensity since the 1999 Bridge ...
The tornado, known as the Greensburg tornado, Greensburg, or GT in later studies, tracked 28.8 miles (46.3 km) through the area, killing eleven and injuring sixty-three others. The tornado was the first to be rated EF5 on the Enhanced Fujita scale after the retirement of the original Fujita scale in the United States on February 1, 2007.
Greensburg, Kansas — — 179 mph (288 km/h) An X-band mobile radar owned by the University of Massachusetts (UMass X-Pol) observed the tornado for roughly 34 minutes after its birth. Recorded winds "exceeding 80 m/s" (179 mph; 288 km/h) were noted roughly 1.5 km above the radar level. [31] EF2 June 5, 2009: Goshen County, Wyoming — — 271 ...
A strange, green blob lurched across a southern Indiana weather radar Wednesday morning. The National Weather Service says it wasn't caused by rain.
Get the Greensburg, PA local weather forecast by the hour and the next 10 days.
The SPC forecast a potential severe weather event, possibly a major outbreak, beginning October 17 across much of central and eastern North America. A moderate risk of severe storms was issued for October 17 across parts of the central U.S. Some activity developed early in the morning of October 17, although no tornadoes were reported.
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A descending reflectivity core (DRC), sometimes referred to as a blob, is a meteorological phenomenon observed in supercell thunderstorms, characterized by a localized, small-scale area of enhanced radar reflectivity that descends from the echo overhang into the lower levels of the storm.